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Cosmic radio noise absorption in the high‐latitude ionosphere during solar wind high‐speed streams
Author(s) -
Grandin M.,
Aikio A. T.,
Kozlovsky A.,
Ulich T.,
Raita T.
Publication year - 2017
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
eISSN - 2169-9402
pISSN - 2169-9380
DOI - 10.1002/2017ja023923
Subject(s) - substorm , riometer , ionosphere , physics , solar wind , geophysics , atmospheric sciences , magnetosphere , local time , astrophysics , plasma , statistics , mathematics , quantum mechanics
The effect of solar wind high‐speed streams (HSSs) on energetic particle precipitation at auroral and subauroral latitudes ( L = 3.8–5.7) is studied by using cosmic noise absorption (CNA) data measured by the Finnish riometer chain during 95 HSS events occurring between 2006 and 2008. The data are divided into “long” and “short” HSS events, depending on whether the maximum solar wind speed is reached within 24 h or later after the arrival of the corotating interaction region (CIR) at the bow shock. We find that CNA is more frequent during long events and extends to subauroral latitudes, unlike during short events. CNA is observed for at least 4 days after the CIR arrival during long events, and only 3 days during short events. In addition, CNA is divided into three categories, depending on whether it is associated with local substorm activity, with ultralow frequency (ULF) wave activity, or neither of these. Substorm‐type CNA dominates in the 21–06 magnetic local time (MLT) sector, while ULF‐type CNA dominates from morning to afternoon and follows the daily S Y M ‐ H index variations. This indicates the importance of having energetic ( E > 30 keV) electrons available for interacting with the very low frequency (VLF) chorus waves, which may be modulated by ULF waves. Finally, we find a correlation between ULF‐type CNA on the dayside and substorm activity on the nightside with a 30 min delay, suggesting that substorm injections energize electrons, which then drift to the morning and dayside, where they precipitate into the ionosphere.